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For governing groundwater, many communities and states follow the English Rule or "Rule of Capture" as it is a robust way to handle the complexities of groundwater flow.

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Final answer:

Groundwater is a significant reservoir of fresh water that flows through pores and fissures in the ground, eventually reaching streams and lakes. Aquifers are being depleted faster than they are being replenished.

Step-by-step explanation:

Groundwater is a significant reservoir of fresh water found in the pores between particles in sand and gravel or in the fissures in rocks. It flows slowly through these pores and fissures, eventually finding its way to a stream or lake where it becomes part of the surface water again. Many streams receive a constant inflow of groundwater, making them flow continuously. Groundwater reservoirs, or aquifers, are the source of drinking or irrigation water and are often being depleted faster than they are being replenished.

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User PinnyM
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